online_blaney_criddle: Potential evapotranspiration by the Blaney-Criddle method. Formulas. p = f(m,L,H) f = p(t + ) · a,b = f(i,RH,w) [ET]o = a + bf. The estimation of potential evapotranspiration is achieved by adopting empirical approaches, such as the Thornthwaite equation, the Blaney-Criddle formula. Notes: Evapotranspiration was calculated using a modified Blaney-Criddle method. Average effective rainfall is the amount that is useful to crops in an average.

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### Blaney–Criddle equation | Revolvy

The crop water need mainly depends on: As can be seen from Table 6 there is a large variation of values not only between crops but also within one crop type. Views Read Edit View history. Just after cutting they are in the “initial stage”, while just before the next cutting, they are in the “late season stage”. There are a large number of theoretical methods to determine the ETo. To determine the crop water need it is best to use an average value of the crop factor Kc.

Member feedback about Evapotranspiration: Water cycle of the Earth’s surface, showing the individual components of transpiration and evaporation that make up evapotranspiration. Notable people with the surname include: When a crop is harvested “green” or “fresh” the late season stage is short. Evapotranspiration Formulas Because of the large number of ET formulas and modifications which exist, any attempt to analyze the most suitable for a particular use requires some selection to limit the cases considered.

Rather than a precise measure of evapotranspirationthe output of the equation is better thought of as providing an order of magnitude [3].

Other approaches to the reference crop concept include a the use of the empirical formulas, without local calibration, as a reference and b the use of pan evaporation. The June and July values would be nearest the definition of an actively growing well-developed alfalfa crop.

If in a local meteorological station the daily minimum and maximum temperatures are measured, the mean daily temperature is calculated as follows: Estimates can vary widely among the various methods and, unfortunately, no definite guidelines are available for defining the model or method of application most likely to give the best estimates.

Allen and John W.

## Blaney–Criddle equation

Thus, these methods are probably preferred for applications such as irrigation scheduling. When sufficient meteorological data is available the Penman—Monteith equation is usually preferred. Indicate on table, as per example below, the ETo values and the duration of the growth stages. The original Blaney-Criddle formula Blaney and Criddle, blanej of the form: Less important is the choice of the various lengths of growth stages. If the pan factor is not known the average value could be used see box.

Field measurements at selected locations are required to calibrate the equations which may then be used to estimate ET o at other locations using climatological data.

After 6 months the Kc value remains constant: Given the coarse accuracy of the Blaney—Criddle equation, it is recommended that it be used to calculate evapotranspiration for periods of one month or greater [1]. If a crop is planted in the winter or is growing in the cool season the total growing period is long. The original Blaney-Criddle uses only a crop growth stage coefficient while the SCS version of the Blaney-Criddle also includes a temperature coefficient k t.

Crop coefficients for the original Jensen-Haise, the modified Jensen-Haise, and the modified Penman equations are given in Table 22 for alfalfa and mountain meadows. In general, those which appear to be most popular in the Western United States are emphasized. This selection process is, admittedly, rather arbitrary and may be dependent as much upon personal experience as scientific criteria. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy interception, and waterbodies.

The crop coefficients represent the effect of the crop characteristics on crop water requirements and are empirically determined values relating ET o to ET m. Cucumber, also fully developed, will use less water than the reference grass crop: SCS TR gives crop growth stage coefficients for alfalfa and pasture grass. The first step is to determine reference crop ET from either field measurements or equations requiring climatological data.

The effects of cutting are not apparent cridde any of the coefficients, although seasonal cycles do exist which reflect the development of the crops during the season.

Rather, it is recommended that, if the equations are used, conversion of input and output data be performed to achieve desired units. The influence of the climate on crop water needs is given by the reference crop evapotranspiration ETo.

This method, however, is rather complicated and beyond the scope of this manual. The ETo is usually expressed in millimetres per unit of time, e. Calibration of the formulas usually involve either or both of two steps. The K pan is low if: The crop thus reaches its full production potential under the given environment.

The formulas considered herein include those ranging from temperature based methods to the more data intensive combination methods. Calculate, on a monthly basis, the crop water need, using the formula: Rice For paddy rice the values indicated in Table 11 should be used. The values should be increased by 0. The influence of the climate is given by the reference crop evapotranspiration ETo; the reference crop used for this purpose is grass see Fig.

In nearly all cases the measured water use rates were lower than the estimated FAO reference crop values.

The difference will be most pronounced for the stage during which the temperature is the lowest. If the sensitivity is high it means that the crop cannot withstand water shortages very well and such shortages should be avoided. Kc and the growth stage of the crop A certain crop will use more water once it is fully developed, compared to a crop which has just recently been planted.

Tables 12a and 12b can be used. Thus, it is necessary to apply crop coefficients to the calculated reference ET rates to estimate alfalfa water use at times when the above conditions do not exist. For example, each morning at 7 o’clock a measurement is taken.